Individual Aerosol Particle Composition Variations in Air Masses Crossing the North Sea

1994 ◽  
Vol 28 (8) ◽  
pp. 1513-1520 ◽  
Author(s):  
Lieve A. De Bock ◽  
Hans. Van Malderen ◽  
Rene E. Van Grieken
2007 ◽  
Vol 7 (13) ◽  
pp. 3481-3495 ◽  
Author(s):  
J. Kusmierczyk-Michulec ◽  
G. De Leeuw ◽  
M. M. Moerman

Abstract. Sun photometer measurements at the AERONET station at the North Sea coast in The Hague (The Netherlands) provide a climatology of optical and physical aerosol properties for the area. Results are presented from the period January 2002 to July 2003. For the analysis and interpretation these data are coupled to chemical aerosol data from a nearby station of the Dutch National Air Quality Network. This network provides PM10 and black carbon concentrations. Meteorological conditions and air mass trajectories are also used. Due to the location close to the coast, the results are strongly dependent on wind direction, i.e. air mass trajectory. In general the aerosol optical properties are governed by industrial aerosol emitted form various industrial, agricultural and urban areas surrounding the site in almost all directions over land. For maritime air masses industrial aerosols are transported from over the North Sea, whereas very clean air is transported from the NW in clean polar air masses from the North Atlantic. In the winter the effect of the production of sea salt aerosol at high wind speeds is visible in the optical and physical aerosol data. In these cases fine and coarse mode radii are similar to those reported in the literature for marine aerosol. Relations are derived between the Ångström coefficients with both the fine/coarse mode fraction and the ratio of black carbon and PM10.


A 15 month survey was carried out into the distributions of trace metals, trace organics and nitrogen species in particulate and rainwater samples collected from the atmosphere over the southern North Sea. This is the first time a comprehensive and reliable data-set of this kind has been obtained for a coastal region from collections made at sea. Trace metals . There is a south-north decrease in the emission of trace metals to the atmosphere from the land masses surrounding the North Sea. ´End-member` aerosol trace metal concentrations have been identified for the three major source regions; i.e. continental Europe, U.K. and the open-sea, and indicate that, in general, aerosols from air masses which have crossed continental Europe are richer in some trace metals (e.g. Zn and Pb) than those from air masses which have crossed the U.K. There are short-term variations in the concentrations of trace metals in aerosols over the North Sea; however, on an integrated long-term basis the concentrations reflect land-based source emission strengths, and increase towards the south of the region. There is also pronounced short term variability in the concentrations of trace metals in rainwaters collected over the North Sea, but separate contributions from marine, crustal and anthropogenic sources can be identified. Atmospheric fluxes contribute substantially to the total inputs of trace metals to the North Sea, with both wet and ‘dry’ deposition processes being important. Particulate trace organics . The distributions of three main hydrocarbon classes were studied; i.e. saturated hydrocarbons ( n -alkanes), PAH (polynuclear aromatic hydrocarbons) and UCM (uncharacterized complex material). Carbon preference indices of n -alkanes suggest that terrestrial sources dominate, with marine sources being insignificant. In terms of air mass origins, trace organic concentrations are ranked in the order: continental Europe > U.K. > open sea. In terms of air mass origins, the concentrations of trace organics and some trace metals (e.g. Zn and Pb) are higher in aerosols having a continental European than U.K. source. However, on the basis of predominant air mass trajectories over the survey period, the major source of both trace organics and trace metals to the North Sea atmosphere was air which had recently crossed over the U.K. Nitrogen species. Compared to the North Atlantic sea water inflow, the atmosphere is a minor source of nitrogen species to the North Sea. However, atmospheric nitrogen inputs constitute at least 25% of the terrestrial inputs, and may provide the dominant source of nitrogen in stratified areas of the North Sea remote from riverine inputs. ‘Wet’ deposition processes dominate the total nitrogen flux to the sea surface, but ‘dry’ deposition of gaseous and particulate species contributes significantly.


1993 ◽  
Vol 22 (4) ◽  
pp. 220-228 ◽  
Author(s):  
J. Injuk ◽  
H. Van Malderen ◽  
R. Van Grieken ◽  
E. Swietlicki ◽  
J. M. Knox ◽  
...  

2007 ◽  
Vol 7 (1) ◽  
pp. 1557-1594 ◽  
Author(s):  
J. Kusmierczyk-Michulec ◽  
G. de Leeuw ◽  
M. M. Moerman

Abstract. Sun photometer measurements at the AERONET station at the North Sea coast in The Hague (The Netherlands) provide a climatology of optical and physical aerosol properties for the area. Results are presented from the period January 2002 to July 2003. For the analysis and interpretation these data are coupled to chemical aerosol data from a nearby station of the Dutch National Air Quality Network. This network provides PM10 and black carbon concentrations. Meteorological conditions and air mass trajectories are also used. Due to the location close to the coast, the results are strongly dependent on wind direction, i.e.~air mass trajectory. In general the aerosol optical properties are governed by industrial aerosol emitted form various industrial, agricultural and urban areas surrounding the site in almost all directions over land. For maritime air masses industrial aerosols are transported from over the North Sea, whereas very clean air is transported from the NW in clean polar air masses from the North Atlantic. In the winter the effect of the production of sea salt aerosol at high wind speeds is visible in the optical and physical aerosol data. In these cases fine and coarse mode radii are similar to those reported in the literature for marine aerosol. Relations are derived between the Ångström coefficients with both the fine/coarse mode fraction and the ratio of black carbon and PM10.


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